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Vindhyan akinites: an indicator of mesoproterozoic biospheric evolution
1Department of Geology, University of Lucknow, Lucknow, India. purnimasrivastava_51@rediffmail.com
Summary
Microfossils of Archaeoellipsoides, from the Mesoproterozoic Kheinjua Formation, indicate early evolution of specialized cyanobacteria. Their presence suggests atmospheric oxygen levels were above 1% during this period.
Area of Science:
- Paleontology
- Microbiology
- Geology
Background:
- Mesoproterozoic microfossil assemblages are typically dominated by cyanobacteria.
- Heterocystous cyanobacteria, like Nostocales and Stigonematales, are rarely reported in these assemblages.
- Akinites of Archaeoellipsoides, representing specialized cyanobacteria, are found in the Mesoproterozoic Kheinjua Formation.
Purpose of the Study:
- To report and characterize Archaeoellipsoides akinites from the Newari locality.
- To establish a minimum date for the evolution of derived cyanobacteria with cell differentiation.
- To correlate microfossil evidence with geochemical data on Mesoproterozoic atmospheric oxygen levels.
Main Methods:
- Paleontological analysis of microfossils.
- Morphological comparison with modern cyanobacteria.
- Integration of fossil data with geochemical evidence.
Main Results:
- Discovery of a wide size range of Archaeoellipsoides akinites, the smallest reported to date.
- These akinites are comparable to modern Anabaena species.
- The fossils suggest the evolution of cyanobacteria capable of marked cell differentiation.
Conclusions:
- The presence of Archaeoellipsoides akinites provides a minimum age for derived cyanobacteria evolution.
- These findings support geochemical evidence of Mesoproterozoic atmospheric oxygen levels >1% of present day.
- Vindhyan akinites indicate significant Mesoproterozoic biospheric evolution and adaptation to oxygenated environments.